Alfred Station Coquinite Member (new name) of Rushford Lake Formation is recognized in the field as a massively bedded coquinite about 6 ft thick or a coquinite, sandstone, mudstone, and shale sequence about 50 ft thick. Occurs about 500 ft below Cuba Formation within a thick sequence of nonfossiliferous shales, sandstones, and siltstones. At type locality occurs within a clearly defined channel about 400 ft wide and 0 ft deep and consists of cross-bedded and flow-rolled coquinites and sandstones. Underlies Rush Creek member (new name). Included in McHenry Valley Substage (new) of Cassadaga Stage. Age is Late Devonian (Chatauquan).
Source: GNU records (USGS DDS-6; Reston GNULEX).
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